Volume 23 Issue 1
Feb.  2017
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ZHANG Shu-wei, YANG Zhen-yu, WANG Xi-sheng, et al., 2017. ANISOTROPY OF MAGNETIC SUSCEPTIBILITY:THEORY AND CASE STUDIES. Journal of Geomechanics, 23 (1): 135-140.
Citation: ZHANG Shu-wei, YANG Zhen-yu, WANG Xi-sheng, et al., 2017. ANISOTROPY OF MAGNETIC SUSCEPTIBILITY:THEORY AND CASE STUDIES. Journal of Geomechanics, 23 (1): 135-140.

ANISOTROPY OF MAGNETIC SUSCEPTIBILITY:THEORY AND CASE STUDIES

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  • Received: 2016-12-06
  • Published: 2017-02-01
  • Anisotropy of magnetic susceptibility (AMS) has been widely utilized to study orientation of magnetic minerals due to the paleo-flow, and direction of magnetic minerals or their recrystallization caused by tectonic stress. We presented the AMS principle and parameters, and studied AMS changes in:(1) two basalt samples (unheated and heated) that have experienced tectonic deformation, with multidomain (MD) titanomagnetite as dominant magnetic minerals, and this is from a previous study; (2) lake sediments that are majorly characterized by MD magnetite. The results show that AMS can sensitively investigate orientation of magnetic minerals.

     

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